The possibility of significant line emission contributing to the 12, 2
5, 60, and 100 mu m infrared emission is explored for the Rosette H Ir
region. We find that the [O III] fine-structure lines in the far-infr
ared contribute significantly (25%-40%) at both 60 and 100 mu m. All o
f the 12 mu m emission is consistent with emission from [S IV] and oth
er lines. The [O IV] line can explain the 25 mu m emission near the ce
ntral cavity but is unable to explain the strength of the 25 mu m emis
sion at more distant lines of sight. Based on the strength of the 25 m
u m emission and the high 60/100 ratio, we conclude that a hot dust co
mponent within the H II region is necessary and that the best candidat
e for this component is ''astronomical'' iron.